nerc.ac.uk

A case-study of land–atmosphere coupling during monsoon onset in northern India

Barton, Emma J. ORCID: https://orcid.org/0000-0001-5945-9244; Taylor, Christopher M. ORCID: https://orcid.org/0000-0002-0120-3198; Parker, Douglas J.; Turner, Andrew G.; Belusic, Danijel; Böing, Steven J.; Brooke, Jennifer K.; Harlow, R. Chawn; Harris, Phil P.; Hunt, Kieran; Jayakumar, A.; Mitra, Ashis K.. 2019 A case-study of land–atmosphere coupling during monsoon onset in northern India [in special issue: INCOMPASS special collection] Quarterly Journal of the Royal Meteorological Society. https://doi.org/10.1002/qj.3538

Before downloading, please read NORA policies.
[img]
Preview
Text
Barton_et_al-2019-Quarterly_Journal_of_the_Royal_Meteorological_Society.pdf - Published Version
Available under License Creative Commons Attribution 4.0.

Download (126MB) | Preview

Abstract/Summary

This article presents a land–atmosphere case‐study for a single day during monsoon onset, incorporating data from a research aircraft, satellite products and model outputs. The unique aircraft observations reveal temperature and humidity contrasts of up to 5 K and 4 g/kg in the planetary boundary layer induced by spatial variations in soil moisture. Both antecedent rain and irrigation were found to be drivers of this atmospheric variability. There is also evidence of soil moisture‐induced mesoscale circulations above some surfaces. This is the first time such responses have been observed in situ over India. Soil moisture‐driven temperature anomalies are larger than those found in previous observational studies in the African Sahel. Moreover, irrigation in the region is extensive, unlike in the Sahel, and has a similar atmospheric effect to antecedent rainfall. This implies that historical changes in irrigation practices are likely to have had an important influence on mesoscale processes within the Indian monsoon. We also examine evidence linking soil moisture and cloud formation. Above wetter soils we observed a suppression of shallow cloud, whilst the initiation of deep convection occurred mostly in areas affected by wet–dry soil moisture boundaries. To investigate the impact of soil moisture heterogeneity on large‐scale wind flow, three model depictions of the day are assessed: the European Centre for Medium‐Range Weather Forecasts ERA‐Interim and ERA5 reanalyses, and a high‐resolution (1.5 km) simulation generated using the Indian National Centre for Medium Range Weather Forecasting regional convection‐permitting Unified Model. We find evidence indicating surface flux uncertainties in the models lead to ∼3.5 hPa anomalies in the monsoon trough. This does affect the simulation of monsoon circulation and rainfall. Better representation of mesoscale land–atmosphere coupling is likely to improve the depiction of convection within weather and climate models over India.

Item Type: Publication - Article
Digital Object Identifier (DOI): https://doi.org/10.1002/qj.3538
CEH Sections/Science Areas: Hydro-climate Risks (Science Area 2017-)
Unaffiliated
ISSN: 0035-9009
Additional Information. Not used in RCUK Gateway to Research.: Open Access paper - full text available via Official URL link.
Additional Keywords: aircraft observations, convection, Indian monsoon, irrigation, land–atmosphere coupling, monsoon trough, planetary boundary layer, soil moisture
NORA Subject Terms: Meteorology and Climatology
Date made live: 30 Apr 2019 11:50 +0 (UTC)
URI: http://nora.nerc.ac.uk/id/eprint/522960

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...